Academic literature on the topic 'Fault plane solution (FPS)'

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Journal articles on the topic "Fault plane solution (FPS)"

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Telesca, L., V. Alcaz, and I. Sandu. "The stress field of Vrancea region from fault plane solution (FPS)." Natural Hazards and Earth System Sciences 11, no. 10 (2011): 2817–20. http://dx.doi.org/10.5194/nhess-11-2817-2011.

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Abstract. The fault plane solutions (FPS) of 247 seismic events were used for stress field investigation of the region. The eigenvectors t, p, b, and moment tensor M components for each FPS were defined and computed numerically. The obtained results confirm the hypothesis of subduction-type intermediate depth earthquakes for the Vrancea seismic region and this may be considered the first approximation of the stress field for the whole of the Vrancea (intermediate depth) region.
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Du, Jing, and Norm R. Warpinski. "Uncertainty in FPSs from moment-tensor inversion." GEOPHYSICS 76, no. 6 (2011): WC65—WC75. http://dx.doi.org/10.1190/geo2011-0024.1.

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Although microseismic monitoring of hydraulic fractures has primarily been concerned with the dimensions, complexity, and growth of fractures or fracture systems, there is an ever-increasing desire to extract more information about the hydraulic-fracturing and/or natural fractures from microseismic data. Source mechanism analysis, which is concerned with deducing details of the failure process from the microseismic waveform data, is, therefore, attracting more attention. However, most of the studies focus more on the moment-tensor inversion than on extracting fault-plane solutions (FPSs) from inverted moment tensors. The FPSs can be extracted from the inverted moment-tensor, but there remains a question regarding how errors associated with the inversion of the moment-tensor affect the accuracy of the FPSs. We examine the uncertainties of FPS, given the uncertainties of the amplitude data, by looking into the uncertainty propagation from amplitude data into the moment-tensor and then into the resultant FPS. The uncertainty propagation method will be demonstrated using two synthetic examples.
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Yilmazer, Mehmet, Bilal Bektas, and Miklos Kozlovszky. "Gridification of regional Fault Plain Solution (FPS)." Earth Science Informatics 3, no. 4 (2010): 239–45. http://dx.doi.org/10.1007/s12145-010-0068-x.

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Ma, Ju, Shuang Wu, Yuan Zhao, and Guoyan Zhao. "Cooperative P-Wave Velocity Measurement with Full Waveform Moment Tensor Inversion in Transversely Anisotropic Media." Sensors 22, no. 5 (2022): 1935. http://dx.doi.org/10.3390/s22051935.

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Precise stochastic approaches to quantitatively calculate the source uncertainties offers the opportunity to eliminate the influence of anisotropy on moment tensor inversion. The effects of ignoring anisotropy were tested by using homogeneous Green’s functions. Results indicate the influence of anisotropy and noise on fault plane rotation is very small for a pure shear source whether it is restricted to double couple solution or full moment tensor solution. Green’s functions with different prior rough anisotropy information were tested, indicating that the complex source is more sensitive to velocity models than the pure shear source and the fault plane rotation caused by full moment tensor solution is larger than the pure double couple solution. Collaborative P-wave velocity inversion with active measurements and passive acoustic emission data using the fast-marching method were conducted, and new Green’s functions established based on the tomography results. The resolved fault plane solution rotated only 3.5° when using the new Green’s functions, but the presence of spurious isotropic and compensated linear vector dipole components was not completely eliminated. It is concluded that the cooperative inversion is capable of greatly improving the accuracy of the fault plane solutions and reducing the spurious components in the full moment tensor solution.
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Wong, Ivan G., and James R. Humphrey. "The 14 August 1983 Cimarron, Colorado Earthquake and the Cimarron Fault." Mountain Geologist 23, no. 1 (1986): 14–18. http://dx.doi.org/10.31582/rmag.mg.23.1.14.

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On 14 August 1983, a small earthquake of Richter magnitude 3.4 occurred near the town of Cimarron in southwestern Colorado. The analysis of data collected from seismographic stations located within the intermountain U.S. suggests the earthquake occurred on the Cimarron fault, a major west-northwest trending Precambrian fault which has experienced displacement possibly since Oligocene time. A fault plane solution determined for the earthquake exhibits normal faulting on a moderately dipping, west-northwest- or east-west-trending fault plane in good agreement with the geologic observations of the Cimarron fault. The fault plane solution also displays a north-northeast trending minimum compressive stress suggesting that this earthquake occurred in response to a reactivation of the Cimarron fault in an extensional tectonic stress field similar to that observed in the Rio Grande rift to the southeast or the Southern Great Plains to the east. The location and the faulting characteristics of the Cimarron earthquake represent the best evidence to date that associates an earthquake with a known major fault in Colorado.
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Eva, Elena, Franco Pettenati, Stefano Solarino, and Livio Sirovich. "The focal mechanism of the 7 September 1920, Mw 6.5 earthquake: insights into the seismotectonics of the Lunigiana–Garfagnana area, Tuscany, Italy." Geophysical Journal International 228, no. 3 (2021): 1465–77. http://dx.doi.org/10.1093/gji/ggab411.

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SUMMARY To understand the seismotectonics and the seismic hazard of the study sector of the Northern Apennines (Italy), one of the most important earthquakes of magnitude Mw = 6.5 which struck the Lunigiana and Garfagnana areas (Tuscany) on 7 September 1920 should be studied. Given the early instrumental epoch of the event, neither geometric and kinematic information on the fault-source nor its fault-plane solution were available. Both areas were candidates for hosting the source fault and there was uncertainty between a normal fault with Apenninic direction or an anti-Apenninic strike-slip. We retrieved 11 focal parameters (including the fault-plane solution) of the 1920 earthquake. Only macroseismic intensity information (from 499 inhabited centres) through the KF-NGA inversion technique was used. This technique uses a Kinematic model of the earthquake source and speeds up the calculation by a Genetic Algorithm with Niching. The result is a pure dip-slip focal solution. The intrinsic ambiguities of the KF-NGA method (±180° on the rake angle; choice of the fault plane between the two nodal planes) were solved with field and seismotectonic evidence. The earthquake was generated by a normal fault (rake angle = 265° ± 8°) with an Apennine direction (114° ± 5°) and dipping 38° ± 6° towards SW. The likely candidate for hosting the source-fault in 1920 is the Compione-Comano fault that borders the NE edge of the Lunigiana graben. The KF-NGA algorithm proved to be invaluable for studying the kinematics of early instrumental earthquakes and allowed us to uniquely individuate, for the first time ever, the seismogenic source of the 1920 earthquake. Our findings have implications in hazard computation and seismotectonic contexts.
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Daniarsyad, Gatut, Aprilia Nur Vita, and Shengji Wei. "Focal Mechanism Analysis of the September 25th, 2019 Mw 6.5 Ambon Earthquake and Its Implication for Seismotectonics." IOP Conference Series: Earth and Environmental Science 873, no. 1 (2021): 012032. http://dx.doi.org/10.1088/1755-1315/873/1/012032.

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Abstract On September 25th, 2019, an Mw 6.5 earthquake occurred in Ambon, Maluku Province, Indonesia, and caused casualties and infrastructures damages. The epicenter located in a tectonically active region with the potential strike-slip and thrust faulting earthquake sources, yet the responsible fault is still not well understood. Based on focal mechanism solutions from available seismological agencies, i.e. USGS, GFZ, GCMT, and BMKG, the earthquake has a similar strike-slip focal mechanism, although there are discrepancies on detailed source parameters. To provide a better understanding of the earthquake mechanism and seismotectonic, we apply the Cut-and-Paste (CAP) focal mechanism inversion method to broadband seismic waveforms from regional and teleseismic distances. The CAP inversion results on the regional data grouped in different distance ranges show a robust strike-slip solution. We then refine the earthquake focal depth by performing the CAPtele inversion and resulted in a depth of 12 km with similar fault plane solution as the regionals. The ruptured fault plane is resolved by a directivity analysis using azimuthal pattern of the apparent source durations, which indicates an obvious unilateral rupture propagation toward SSE direction. Our result suggests the NNW-SSE orientated fault is the ruptured fault plane, which is also consistent with the near N-S distributed aftershocks. This fault is located in a narrow sea between Seram, Ambon and Haruku island and was not reported yet in previous studies. The Coulomb failure stress (CFS) changes analysis of the mainshock shows that the Ambon earthquake has promoted the off-fault aftershocks which occurred to the west of the ruptured fault.
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Kiratzi, Anastasia A., and Constantinos B. Papazachos. "Moment-tensor summation to derive the active crustal deformation in Japan." Bulletin of the Seismological Society of America 86, no. 3 (1996): 821–31. http://dx.doi.org/10.1785/bssa0860030821.

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Abstract The country of Japan and the surrounding area has been divided into 12 seismogenic sources, which belong to five belts with an almost uniform orientation of the stress field. In each one of these sources, the active crustal deformation has been determined, using the summation of the seismic moment tensors of mainly post-1964 earthquakes. The analysis showed that due to the subduction of the Philippine Sea plate beneath the Eurasian plate, the deformation is expressed as compression at a mean direction of N53°W and an average rate of 1.5 cm/yr. The fault-plane solution corresponding to the summed tensor indicates low-angle thrust faulting with the following parameters: strike 226°, dip 21°, and rake 98°. Along the Sagami trough, dextral strike-slip motion is predominant at an average rate of 6 cm/yr. The summed tensor corresponds to a fault-plane solution with strike 291°, dip 73°, and rake 180°. Along the districts of Fukushima, Tohoku, and the Hokkaido Island, the motion of the Pacific plate toward Eurasia causes compression at a mean direction of N65°W and an average rate of 4 cm/yr. The summed tensor corresponds to a fault-plane solution with strike 199°, dip 18°, and rake 81°, that is, low-angle thrust faulting dipping toward the land. This pattern resembles the Hellenic arc, where the deformation is also taken up by motion on low-angle (18°) thrust faults dipping to the north. In the Tohoku district, the rate of motion reaches a value of 8 cm/yr, which is the highest calculated in the whole Japan area. In the inner part of the Japanese islands (along western Honshu and Niigata), the mean P axis is almost horizontal, trending nearly E-W. In western Honshu, the deformation is mainly expressed as dextral strike-slip motion at an average rate of 5 cm/yr in a N59°E direction. The representative fault-plane solution for this area has strike 240°, dip 81°, and rake 173°. At Niigata, the western coast of Hokkaido, and further north at Okushiri, the deformation is taken up as compression at a mean direction of N96°E at an average rate of 2 cm/yr. The summed tensor corresponds to a fault-plane solution with strike 5°, dip 41°, and rake 90°. The calculated directions and rates of motion along the Japanese islands are in good agreement with the expected values from plate-motion models.
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Hasegawa, Henry S., and John Adams. "Reanalysis of the 1963 Baffin Island Earthquake (MS 6.2) and its Seismotectonic Environment." Seismological Research Letters 61, no. 3-4 (1990): 181–92. http://dx.doi.org/10.1785/gssrl.61.3-4.181.

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Abstract The 1963 Baffin Island earthquake of MS 6.2 is reanalyzed to determine whether or not it involved normal faulting, as previously suggested. The revised fault-plane solution has nodal planes with strike 113°, dip 66°, rake 235° and strike 352°, dip 41°, rake 322°. The T-axis trends 227° and plunges 14°, and the P-axis trends 338° and plunges 55°. Thus though this solution confirms normal faulting, it suggests a larger strike-slip component than most previous studies. The tension axis is oriented SW, which is normal to the NW geographic trend of Baffin Island. We consider that the normal-fault regime could be a transient phenomena related to extensional stress in the glacial forebulge presently centered over northeast Baffin Island, and is associated with incomplete postglacial rebound. However, future geophysical measurements such as heat flow, in-situ stress and vertical uplift rate, as well as more fault-plane solutions are required to test this hypothesis.
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Torres-Contreras, Ignacio, Juan Carlos Jáuregui-Correa, Carlos Santiago López-Cajún, and Salvador Echeverría-Villagómez. "Effects of Phase Shift Errors in Recurrence Plot for Rotating Machinery Fault Diagnosis." Applied Sciences 11, no. 2 (2021): 873. http://dx.doi.org/10.3390/app11020873.

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For fault diagnosis and predictive maintenance of rotating machinery, the phase errors generated by the integration processing of a vibration signal are an essential investigation subject. Phase errors affect the solution of mechanical systems with multiple vibration sources and also the information transmitted through the vibration that is used for fault diagnosis. This work proposes the use of phase plane, recurrence plot (RP), and cross recurrence plot (CRP) to evaluate phase shift error effects on the solution of multiple asynchronous and simple periodic functions, and on the smoothing of a Gaussian peak with white noise. Noisy peaks were smoothed twice with the triangular method and with a different number of points. The analysis of the asynchronous periodic functions and the smoothing indicated that a small phase shift changes the phase plane and the RP pattern. These changes can affect not only the accuracy of machinery fault diagnosis but also prediction for the application of timely maintenance actions.
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Dissertations / Theses on the topic "Fault plane solution (FPS)"

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Kaplan, Tulin. "Neotectonics And Seismicity Of The Ankara Region: A Case Study In The Urus Area." Master's thesis, METU, 2004. http://etd.lib.metu.edu.tr/upload/12605238/index.pdf.

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Study area, the UruS province, is located 70 km WNW of city of Ankara. Major settlements in the study area are two counties, UruS and G&uuml<br>d&uuml<br>l<br>and there are a number of villages, such as, from W to E, Macun, Yogunpelit, Kabaca, &Uuml<br>regil, &Ouml<br>zk&ouml<br>y, Tahtaci&ouml<br>rencik, Kirkkavak, Kavak&ouml<br>z&uuml<br>, Kayi and Karaca&ouml<br>ren. The study area is 189 km2 in size and included in 1/25000-scaled topographic quadrangles of H28a3, a4, d1 and d2. The G&uuml<br>d&uuml<br>l- UruS section of the &Ccedil<br>eltik&ccedil<br>i morphotectonic depression (&Ccedil<br>eltik&ccedil<br>i Basin) drained by the Antecedent Kirmir River and its second-order drainage system was first mapped in detail in the present study, and faults determining northern margin of the &Ccedil<br>eltik&ccedil<br>i depression were named as the UruS fault set comprising the SW part of the &Ccedil<br>eltik&ccedil<br>i Fault Zone<br>and the mechanism of the master fault of the UruS fault set was determined as left lateral oblique-slip fault with reverse component by the morphologic markers such as the deformed drainage system and pressure ridges. This was also supported by the fault plane solutions of the 2000.08.22 UruS earthquake. Three fault plane solutions, of which two of them for the 2000.08.22 UruS earthquake, and one of them for the 2003.02.27 &Ccedil<br>amlidere earthquake, were done to determine nature of the source. Ground material underlying the city of Ankara were divided into three categories: (a) well-lithified basement rocks, (b) Pliocene fluvio-lacustrine v sedimentary sequence, and (c) unconsolidated terrace and alluvial sediments of Quaternary age. Quaternary unconsolidated sediments are densely populated in Ankara. These sediments are fine-grained and have a maximum thickness of 200 m or more. Inside these sediments, static ground water level is very close (as on average: 6 m) to ground surface. These conditions are quite suitable for liquefaction of these unconsolidated alluvial sediments. In addition, basement rocks are full of zone of weakness. Even if, the city of Ankara is characterized by the shallow focus and small earthquakes (M&amp<br>#8804<br>5), it is open to the risk of large earthquakes to be sourced from the North Anatolian Fault System and the Seyfe Fault Zone located 110 km and 80 km, respectively, owing the ground material conditions beneath the city of Ankara. This point has to be taken out in constructions and site selection solution.
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Book chapters on the topic "Fault plane solution (FPS)"

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Mahto, Pooja, and S. C. Gupta. "December 01, 2020, Haridwar, Earthquake: Fault Plane Solution and Tectonic Implications." In Lecture Notes in Civil Engineering. Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-99-1459-3_53.

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"fault-plane solution." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_60386.

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Conference papers on the topic "Fault plane solution (FPS)"

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Kearney, Ian, and Mark Dipsey. "Trends in Discrete Power MOSFET and Power System In-Package Fault Isolation." In ISTFA 2017. ASM International, 2017. http://dx.doi.org/10.31399/asm.cp.istfa2017p0419.

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Abstract Photoluminescence, defect-band emission, and Lock-in Infrared Thermography (LIT) generally enable the correlation of multi-crystalline silicon defect types. Long Wavelength Infrared (LWIR) thermal imaging has traditionally seen limited application in failure analysis. LWIR cameras are typically uncooled systems using a microbolometer Focal Plane Arrays (FPA) commonly used in industrial IR applications, although cooled LWIR cameras using Mercury Cadmium Tellurium (MCT) detectors exists as well. On the contrary, the majority of the MWIR cameras require cooling, using either liquid nitrogen or a Stirling cycle cooler. Cooling to approximately −196 °C (77 K), offers excellent thermal resolution, but it may restrict the span of applications to controlled environments. Recent developments in LWIR uncooled and unstabilized micro-bolometer technology combined with microscopic IR lens design advancements are presented as an alternative solution for viable low-level leakage (LLL) defect localization and circuit characterization. The 30 micron pitch amorphous silicon type detector used in these analyses, rather than vanadium oxide (VOx), has sensitivity less than 50mK at 25C. Case studies reported demonstrate LWIR enhanced package-level and die-level defect localization contrasted with other quantum and thermal detectors in localization systems.
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Berentsen, C. W. J., and C. J. de Pater. "Accurate 2D Modeling of Fault Instability Due to Cold Fluid Injection in CO2 Storage or Geothermal Doublets." In SPE Europe Energy Conference and Exhibition. SPE, 2025. https://doi.org/10.2118/225524-ms.

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Abstract Two-dimensional plane strain models are used frequently to evaluate depletion induced fault instability in permeable reservoirs. However contrary to depletion induced fault instability thermal stress induced fault instability by cold fluid injection is local in nature and the applicability of plane strain models is not straightforward. This paper investigates (A) the accuracy of two-dimensional plane strain (2D-PS) models to evaluate thermal-stress induced fault instability and (B) the requirement to correct elastic solutions for the occurrence of excessive tensile stress. Similar to depletion induced compaction, shear stress significantly contributes to the initial fault criticality ahead of a cold front causing contraction (Stage 1). Only after the cold front intersects with a fault (Stage 2), fault criticality is completely dominated by normal stress reduction. Compared to a full 3D model, a two-dimensional Plane Strain model slightly exaggerates the onset of fault criticality during stage 1 as it gives higher maximum principal and shear stress ahead of the cold front. During stage 2, Plane strain models overpredict horizontal stress arching above and below a thermally compacting body compared to full 3D, which may result in some slight underprediction at intermediate times. However, with a growing cold front in time the deviation converges as the transition from critical to stable occurs at the same depth around the horizontal center axis of the cold front. For increased elongation of the 3D cold front along the constant-axis of the plane strain model, plane strain model results converge to the full 3D model results while the deviation between elastic and tensile stress corrected models converges to a constant offset. Overall, Plane strain models that are corrected for excessive tensile stress provide an efficient but slightly conservative method to access full 3D fault stability behavior by cooling. In case of severe thermal stress reduction, excessive tensile stress has to be compensated because the elastic solution will exaggerate the onset and magnitude of fault criticality as it gives too low minimum principal stress and too high shear stress.
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Liao, Changlin, Ruifeng Wang, Juntao Zhang, et al. "Well Testing Analysis Methodology and Application for Complex Fault-Block reservoirs in the Exploration Stage." In Gas & Oil Technology Showcase and Conference. SPE, 2023. http://dx.doi.org/10.2118/214186-ms.

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Abstract A complex fault-block reservoir usually has large layer span, many thin layers and oil-water systems. The available data are limited in the exploration stage. One of the biggest advantages is that each well is tested several times. Based on comprehensive geological study, this paper proposed a well testing analysis methodology to carry out reservoir evaluation, and the results are applied to the oilfield development plan. Well testing can reflect the static and dynamic characteristics of reservoir at the same time. It shows high application value in the exploration stage. The analysis methodology of well testing in complex fault-block oilfield mainly includes three aspects: (1) Establish a novel calculation method to obtain crude oil parameters of all tested intervals, which are necessary in well test interpretation. (2) Build reliable interpretation models to evaluate wellbore, formation property, productivity and boundary according to pressure derivatives curves. (3) Propose a concise evaluation process to show reservoir characteristics in both vertical and plane. This methodology is applied in Doseo Oilfield and proved to be a great methodology in complex fault-block reservoirs. The calculated crude oil parameters are good matched with limited PVT data. The errors are less than 10%. The formation characteristics obtained from the models including permeability, faults and aquifer energy are well verified by seismic and well-logging interpretation. The reservoirs in middle area on the plane and Zone K in the vertical show high productivity and permeability. They can be selected as the key oil regions for the first production. Similar formation characteristics are reflected by the analogous shape of pressure derivatives. They can be put into production with the same development methods to obtain higher benefits. The innovation is that this paper proposes an analysis methodology of well testing to calculate right crude oil parameters, identify formation characteristics and key oil regions, and find similar reservoirs. It can decrease the errors which are caused by parameter uncertainties and multi-solution of interpretation models.
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Arcano, N. S., B. Vicuna, D. Criollo, et al. "Advanced Gas Analysis Meets Geoscience Solution in Norway Field: The Insights of a Holistic Approach." In ADIPEC. SPE, 2024. http://dx.doi.org/10.2118/222077-ms.

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Abstract Equinor has a complex faulted field in Norway with expected different fluid contacts. To maximize the reservoir understanding a geoscience approach is applied for this project. The utilization of Ultra Deep Azimuthal Resistivity (UDAR) technologies is typically sufficient to control the vertical and lateral limits of a reservoir and unveil potential flooded intervals and oil water contacts (OWC). However, the differentiation between oil and gas by just LWD and UDAR data is not possible. This study demonstrates three geoscience areas contributing for early decision making while drilling the Brent Group formation. The cost-effective solution in this project was the implementation of advanced mud gas (AMG) using a constant volume and constant temperature (CVCT) extractor with advanced gas chromatograph to analyze species such as methane to octane. Correction for recycling gas and extraction efficiency correction (EEC) of methane to pentane species were also applied in real time (RT). The gas ratios curves were the first look of the PVT for this well, therefore the gas oil ratio (GOR) prediction based on the model proposed by Yang et al., 2019 were also available and provide reservoir insight while drilling. The High-Resolution ultrasonic image tool was used to detect bedding, fractures and faults planes post-drilling, and in conjunction to UDAR results several diagrams such as Stereonet plot and curtain sections were displayed. Additionally, an ultrasonic caliper tool was used to identify the borehole shape. The sandstone bedding plane orientation showed several trends inside the whole interval and most of these changes were associated with faulted intervals and validated with Geosteering inversion model. The fault system understanding is important in this basin since it contains a western graben created by several faults stepping down preserving Upper Brent. Petrophysical analysis complements and supports the results from AMG, UDAR and borehole image analysis. The basin setup is helpful to understand the fluid distribution in the petroleum system. From a petrophysical viewpoint, water saturation from resistivity logs and neutron-density separation helped to estimate fluid types, and it was validated with AMG. The identification of 300m of water flushed zone, later confirmed by production, shows the holistic methodology implementation allowed a review of the fluid distribution in the well results. This paper demonstrates the contribution of the race to digital transformation and enabled reservoir characterization while drilling.
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Hu, Jialiang, Pradeep Menon, Amna Al Yaqoubi, et al. "Fracture Characterization in Deep Gas Reservoirs to Identify Fracture Enhanced Flow Units, Offshore Abu Dhabi." In Abu Dhabi International Petroleum Exhibition & Conference. SPE, 2021. http://dx.doi.org/10.2118/207646-ms.

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Abstract High gas flow rates in deep-buried dolomitized reservoir from an offshore field Abu Dhabi cannot be explained by the low matrix permeability. Previous permeability multiplier based on distance to major faults is not a solid geological solution due to over-simplifying reservoir geomechanics, overlooking folding-related fractures, and lack of detailed fault interpretation from poor seismic. Alternatively, to characterize the heterogeneous flow related with natural fractures in this undeveloped reservoir, fracture network is modelled based on core, bore hole imager (BHI), conventional logs, seismic data and test information. Limited by investigation scale, vertical wells record apparent BHI, and raw fracture interpretation cannot represent true 3D percolation reflected on PLT. To overcome this shortfall, correction based on geomechanics and mechanical layer (ML) analysis is performed. Young's modulus (E), Poisson ratio (ν), and brittleness index are calculated from logs, describing reservoir tendency of fracturing. Other than defining MLs, bedding plane intensity from BHI is also used as an indicator of fracture occurrence, since stress tends to release at strata discontinuity and forms bed-bounded fractures observed from cores. Subsequently, a new fracture intensity is generated from combined geomechanics properties and statistics average of BHI-derived fracture occurrence within the ML frame, which improves match with PLT and distinguishes fracture enhance flow intervals consistently in all wells. Seismic discontinuity attributes are used as static fracture footprints to distribute fractures from wells to 3D. The final hybrid DFN comprises large-scale deterministic zone-crossing fractures and small-scale stochastic bed-bounded fractures. Sub-vertical open fractures are dominated by NE-SW wrenching fractures related with Zagros compression and reactive salt upward movement. There is no angle rotation of fractures in different fault blocks. Open fractures in other strikes are supported by partial cements and mismatching fracture walls on computerized tomography (CT) images. ML correlation shows vertical consistence across stratigraphic framework and its intensity indicates fracture potential of vertical zones reflected by tests. Fracture-enhanced flow units are further constrained by a threshold in both combined geomechanics properties and statistics average of raw BHI fracture intensity in ML frame. As a result, final fracture network maps reservoir brittleness and flow potential both vertically and laterally, identifying fracture regions along folding axis not just major faults, evidenced by wells and seismic. According to the upscaling results, the case study reveals a type-III fractured reservoir, where fractures contribute to flow not to volume. Fracture network enhances bed-wise horizontal communication but also opens vertical feeding channels. Fracture permeability is mainly influenced by aperture and intensity, while aspect ratio, fracture length, and proportion of strikes and dips mainly influence permeability distribution rather than absolute values. This study provides a production-oriented characterization workflow of natural fracture heterogeneity based on correction of raw BHI in undeveloped fields.
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